Measurement range of E-Ex and E-Eφ wide field electromagnetic methods
Li Diquan1,2,3
1. Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Ministry of Education, Central South University, Changsha, Hunan 410083, China; 2. Hunan Key Laboratory of Nonferrous Resources and Geological Hazard Detection, Changsha, Hunan 410083, China; 3. School of Geosciences and Info-Physics, Central South University, Changsha, Hunan 410083, China
Abstract:WFEM electromagnetic field intensity and apparent resistivity curves suffer serious distortions,when its measurement exceed the range of -30°~30° in the perpendicular direction and the range of -20°~20° in the axial direction of the dipole.So its measurement range should be redefined.Using half space model for numerical simulation,we analyze the variation of the antenna direction,EM field,and apparent resistivity with the angle,and discuss E-Ex and E-Eφ measurement range.Based on our research,the best measurement range for E-Ex WFEM covers 30° area of the both sides of the perpendicular direction and 20° area of both sides in the axial direction of the dipole; the best measurement range for E-Eφ WFEM is 60° area on the both sides in the perpendicular direction of the dipole.For E-Ex WFEM,the broadside line length is about 1.15 times of the vertical offset; and for E-Eφ WFEM,the line length is up to 3.46 times of the vertical offset.It is suggested to use E-Ex WFEM on 30° area of both sides in the perpendicular direction and 20° area of both sides in the axial direction of the dipole,and use E-Eφ WFEM on 30°~60° area of both sides in the perpendicular direction.
李帝铨. E-Ex和E-Eφ广域电磁法测量范围[J]. 石油地球物理勘探, 2017, 52(6): 1315-1323.
Li Diquan. Measurement range of E-Ex and E-Eφ wide field electromagnetic methods. Oil Geophysical Prospecting, 2017, 52(6): 1315-1323.
何继善.广域电磁测深法研究.中南大学学报(自然科学版),2010,41(3):1065-1072.He Jishan.Wide field electromagnetic sounding me-thods.Journal of Central South University(Science and Technology),2010,41(3):1065-1072.
[3]
Goldstein M,Strangway D W.Audio-frequency magnetotellurics with a grounded electric dipole source.Geophysics,1975,40(4):669-683.
[4]
Cagniard L.Basic theory of the magnetotelluric method of geophysical prospecting.Geophysics,1953,18(3):605-635.
[5]
Tikhonov A.On determining electrical characteristics of the deep layers of the earth's crust.Nauk SSSR,1950,73:295-297.
[6]
何继善,佟铁钢,柳建新.an序列伪随机多频信号数学分析及实现.中南大学学报(自然科学版),2009,40(6):1666-1671.He Jishan,Tong Tiegang,Liu Jianxin.Mathematical analysis and realization of an sequence pseudo-random multi-frequencies signal.Journal of Central South University (Science and Technology),2009,40(6):1666-1671.
[7]
何继善.三元素集合中的自封闭加法与2n系列伪随机信号编码.中南大学学报(自然科学版),2010,41(2):632-637.He Jishan.Closed addition in a three-element set and 2n sequence pseudo-random signal coding.Journal of Central South University (Science and Technology),2010,41(2):632-637.
[8]
张振宇,王刚,胡祥云等.张量CSAMT方法及对比实验.石油地球物理勘探,2017,52(4):869-874.Zhang Zhenyu,Wang Gang,Hu Xiangyun et al.Tensor CSAMT technical research and experiments.OGP,2017,52(4):869-874.
[9]
严波,李予国,韩波等.任意方位电偶源的MCSEM电磁场三维正演.石油地球物理勘探,2017,52(4):859-868.Yan Bo,Li Yuguo,Han Bo et al.3D marine controlled-source electromagnetic forward modeling with arbitrarily orientated dipole source.OGP,2017,52(4):859-868.
[10]
朱成,李桐林,杨海斌等.带地形频率域可控源电磁法三维反演研究.石油地球物理勘探,2016,51(5):1031-1039.Zhu Cheng,Li Tonglin,Yang Haibin et al.3D controlled source electromagnetic inversion with topography in the frequency domain.OGP,2016,51(5):1031-1039.
[11]
王宏宇.广域电磁法探测含油富集区试验研究[学位论文].湖南长沙:中南大学,2013.
[12]
彭勇辉,李帝铨.柴达木盆地某油气聚集区电性结构研究.岩性油气藏,2015,27(1):115-121.Peng Yonghui,Li Diquan.Study on electric structure in a hydrocarbon accumulation area,Qaidam Basin.Lithologic Reservoirs,2015,27(1):115-121.
[13]
何继善,李帝铨,戴世坤.广域电磁法在湘西北页岩气探测中的应用.石油地球物理勘探,2014,49(5):1006-1012.He Jishan,Li Diquan,Dai Shikun.Shale gas detection with wide field electromagnetic method in Northwestern Hunan.OGP,2014,49(5):1006-1012.
戴世坤,王顺国,张钱江等.频率域可控源电磁法2.5D正反演.中国有色金属学报,2013,23(9):2513-2523.Dai Shikun,Wang Shunguo,Zhang Qianjiang et al.2.5D forward and inversion of CSEM in frequency domain.The Chinese Journal of Nonferrous Metals,2013,23(9):2513-2523.
[16]
凌帆,朱裕振,周明磊等.广域电磁法在南华北盆地长山隆起页岩气资源潜力评价中的应用.物探与化探,2017,41(2):369-376.Ling Fan,Zhu Yuzhen,Zhou Minglei et al.Shale gas potential assessment of Changshan uplift area in southern North China basin by using wide field electromagnetic method.Geophysical and Geochemical Exploration,2017,41(2):369-376.
[17]
杨松霖,袁博,李帝铨.高陡双复杂地区多种页岩气勘探方法效果对比.物探与化探,2016,40(5):941-946.Yang Songlin,Yuan Bo,Li Diquan.An analysis of some different exploration methods in complex terrain area.Geophysical and Geochemical Exploration,2016,40(5):941-946.
[18]
符超,袁博,李学兰等.广域电磁法在保靖页岩气勘探中的应用.工程地球物理学报,2016,13(4):416-422.Fu Chao,Yuan Bo,Li Xuelan et al.The exploration of wide field electromagnetic method on shale gas.Chinese Journal of Engineering Geophysics,2016,13(4):416-422.
[19]
郑冰,李帝铨.广域电磁法和大地电磁法在中国南方某页岩区块的对比试验.油气地球物理,2015,13(3):45-49.Zheng Bing,Li Diquan.Comparative test of wide field electromagnetic method and MT at a shale gas blockin the south of China.Petroleum Geophysics,2015,13(3):45-49.
[20]
李昭,刘海军,张生等.TFEM油气检测技术及其在伊犁盆地的应用.石油地球物理勘探,2017,52(2):398-401.Li Zhao,Liu Haijun,Zhang Sheng et al.Hydrocarbon detection with TFEM in Yili Basin,China.OGP,2017,52(2):398-401.
[21]
王志刚,何展翔,覃荆城等.时频电磁技术的新进展及应用效果.石油地球物理勘探,2016,51(增刊):144-151.Wang Zhigang,He Zhanxiang,Qin Jingcheng et al.Advances of TFEM technique and its application.OGP,2016,51(S):144-151.
[22]
李燕丽,金凤鸣,魏强等.时频电磁法在冀中坳陷潜山及潜山内幕油气预测中的应用.石油地球物理勘探,2016,51(增刊):137-143.Li Yanli,Jin Fengming,Wei Qiang et al.Hydrocarbon prediction with TFEM in buried hills,Jizhong Depression.OGP,2016,51(S):137-143.
[23]
何继善.可控源音频大地电磁法.湖南长沙:中南工业大学出版社,1990.
[24]
底青云,王若.可控源音频大地电磁数据正反演及方法应用.北京:科学出版社,2008.
[25]
汤井田,何继善.可控源音频大地电磁法及其应用.湖南长沙:中南大学出版社,2005.
[26]
Nabighian M N.Electromagnetic Methods in Applied Geophysics.SEG,1988,9-29.